Record Details
Field | Value |
---|---|
Title | page 2273 |
Relation | gov serial set 1955 |
Date | 2005-10-24 to 2005-10-26 |
Rights | This item is in the public domain. Acknowledgement of the University of Oregon Libraries as a source is requested. |
Type | page |
Format | Scanned from originals using Silverfast AI 6.0 on UMAX Powerlook III flatbed scanner. Scanned images saved as 16 bit grayscale tiffs. 273.972 kb 8 bit - Gray Gamma 2.2 - greyscale Omnipage 14 used to OCR 8 bit tiffs and generate text files for full text access. 16 bit grayscale and 48>24 RGB color tiffs edited in Photoshop CS 8.0: cropped, rotated, reduced in size, levels adjusted, grayscale bit depth reduced to 8 and JPEGs created. |
Description | sediment by the Columbia flood, which varies in depth from 2 to 4 feet, will not extend above the plane of 20 feet below low-water level; and that the fresh deposits being soft and easily eroded will, instead of remaining to build up the bars in layers, consolidating with the pressure of yearly accretions, be carried off almost as fast as the flood abates by the outward currents of the river and ebb-tides, which will increase in volume and force with the general deepening of the channel.... |
Identifier | http://oregondigital.org/u?/wwdl,3253 |